IGRINS Science Workshop 2010 1 High Spectral Resolution Mid- Infrared Spectroscopy as a Probe of the Physical State of Planetary Atmospheres August 26,

Slides:



Advertisements
Similar presentations
The Atmosphere.
Advertisements

Basics & Motivation Technique & Observations Fits & Measurements Summary & Outlook Atmospheric Wave Workshop ESTEC 11/10/2011 Tobias Stangier I st Physics.
Spectro-imaging observations of H 3 + on Jupiter Observatoire de Paris, France Emmanuel Lellouch.
Colors of Alien Worlds from Direct-Imaging Exoplanet Missions Renyu Hu Hubble Fellow Jet Propulsion Laboratory California Institute of Technology With.
8/28/2002 Ozone Abundance in Earth-like Planets NTNU Earth Science Department Shung-wen Hsu Supervisor : Gu, Pin-Gao.
Oxygen: Stratosphere, Mesosphere and Thermosphere Part-3 Chemical Rate Equations Ozone Density vs. Altitude Stratospheric Heating Thermal Conductivity.
Propane on Titan H.G. Roe 1, T. Greathouse, M. Richter, J. Lacy 1 Div. Of Geological and Planetary Sciences, CalTech Roe, H. et al. 2003, ApJ, 597, L65.
Reflection Spectra of Giant Planets With an Eye Towards TPF (and EPIC & ECLIPSE) Jonathan J. Fortney Mark S. Marley NASA Ames Research Center 2005 Aspen.
METO 637 Lesson 22. Jupiter Jupiter and Saturn are known as the gas planets They do not have solid surfaces, their gaseous materials get denser with.
Molecules in planetary atmospheres Emmanuel Lellouch Observatoire de Paris.
Lecture 14: Searching for planets orbiting other stars III: Using Spectra 1.The Spectra of Stars and Planets 2.The Doppler Effect and its uses 3.Using.
Hydrogen Peroxide on Mars Th. Encrenaz 1, B. Bezard, T. Greathouse, M. Richter, J. Lacy, S. Atreya, A. Wong, S. Lebonnois, F. Lefevre, F. Forget 1 Observatoire.
RECENT ADVANCES IN THE SPECTROSCOPY OF PLANETARY AND EXOPLANETARY ATMOSPHERES : WHAT IS OUT THERE ? Hitran 2010 Pierre Drossart LESIA, Observatoire de.
A Warm South Pole? Yes, on Neptune! A&A 473, L5 – L8 (2007) "Evidence for Methane Escape and Strong Seasonal and Dynamical Perturbations of Neptune's Atmospheric.
AOSC 637 Lesson 24. Uranus Has been visited by Voyager 2 in Plane spins on an axis almost parallel to the ecliptic plane. Polar regions can point.
Detecting molecules in the atmospheres of transit Exoplanets Giovanna Tinetti University College London Mao-Chang Liang Academia Sinica, Taiwan.
Infrared spectroscopy of Hale-Bopp comet Rassul Karabalin, Ge/Ay 132 Caltech March 17, 2004.
Deuterated Methane and Ethane in the Atmosphere of Jupiter Christopher D. Parkinson 1,2, Anthony Y.-T. Lee 1, Yuk L. Yung 1, and David Crisp 2 1 Division.
7/2/2015Richter - UC Davis1 EXES, the echelon-cross-echelle spectrograph for SOFIA Matthew J. Richter (UC Davis) with Mark McKelvey (NASA Ames Research.
Outline Further Reading: Chapter 05 of the text book - continental vs. marine regimes - temperature structure of the atmosphere - seasonal variations Natural.
Meridional Mapping of Mesospheric Temperatures from CO 2 Emission along the MGS Ground Track T. A. Livengood 1, T. Kostiuk, K. E. Fast, J. N. Annen, G.
Mid-Infrared Ethane Emission on Neptune and Uranus Heidi B. Hammel, M. Sitko (Space Science Inst.) D. Lynch, R. Russell (The Aerospace Corp.), L.S. Bernstein.
بسم الله الرحمن الرحيم. Atmospheric pressure  Atmosphere: The earth is surrounded by a gas envelope that rotates with it about its axis, and extends.
Figure 1 Figure 8 Figure 9Figure 10 Altitude resolved mid-IR transmission of H 2 O, CH 4 and CO 2 at Mauna Loa Anika Guha Atmospheric Chemistry Division,
ALMA Science Workshop, May 2004 Solar System Science with the ALMA Mark Gurwell Harvard-Smithsonian Center for Astrophysics ALMA Science Workshop, May.
Atmospheric temperature
INTRODUCTION TO GEOPHYSICS AND SPACE SCIENCE Günter Kargl Space Research Institute Austrian Academy of Sciences WS 2013.
ATMOSPHERE.
Observing Solar System Objects with JWST Dr. Heidi B. Hammel AURA (Washington, DC) & Space Science Institute (Boulder, CO)
A Night at the IRTF. Answer the following questions on a scale of 1-4  1. I know nothing about this  2. I know a little about this  3. I know some.
Abundances in the solar system: what we achieved and how much was it dependent on space probes? Sandrine VINATIER LESIA, Observatoire de Paris-Meudon.
SOFIA - Planetary System “Awesome” Science Panel membership Approximate panel schedule Planetary science categories Some science examples - solar system.
Searching for Brown Dwarf Companions to Nearby Stars Michael W. McElwain, James E. Larkin & Adam J. Burgasser (UC Los Angeles) Background on Brown Dwarfs.
ESS 111 – Climate & Global Change
Emily L. Schaller April 28, 2008 II. Volatile Ices on Outer Solar System Objects I. Seasonal Changes in Titan’s Cloud Activity.
General Circulation Modelling on Triton and Pluto
Seasonal Change in Titan’s Cloud Activity (A Titan Weather report) Emily Schaller (Caltech) Mike Brown (Caltech), Henry Roe (Lowell Observatory)
H 3 + and the Planets Steve Miller H the driver of planetary atmospheres.
Atmosphere: Structure and Temperature Bell Ringers:  How does weather differ from climate?  Why do the seasons occur?  What would happen if carbon.
Light. Review Question What is light? Review Question How can I create light with a magnet?
ALMA Science Examples Min S. Yun (UMass/ANASAC). ALMA Science Requirements  High Fidelity Imaging  Precise Imaging at 0.1” Resolution  Routine Sub-mJy.
LINE BY LINE SPECTRAL PARAMETERS IN THE 4nu3 SPECTRAL REGION OF METHANE D. CHRIS BENNER, V. MALATHY DEVI, College of William and Mary J. J. O’BRIEN, S.
Solar System observations with APEX Observatoire de Paris, France Emmanuel Lellouch.
Chapter 23 The Atmosphere Section 1 Characteristics of Atmosphere Notes 23-2.
Clouds in the Tropics of Titan Emily Schaller Lunar and Planetary Laboratory, University of Arizona 2010 Hubble Fellows Symposium.
The Atmosphere: Structure and Temperature
Saturn’s Satellites. Discussion What does the density of Saturn’s satellites tell you about their composition?
Atmosphere. What makes up our atmosphere?  Nitrogen  Oxygen  Argon.
Climate and Global Change Notes 17-1 Earth’s Radiation & Energy Budget Resulting Seasonal and Daily Temperature Variations Vertical Temperature Variation.
Atmosphere Layers. Vertical Structure of the Earth’s Atmosphere Vertical temperature (T) profile: troposphere stratosphere mesosphere Thermosphere (contains.
Composition of the Atmosphere 14 Atmosphere Characteristics  Weather is constantly changing, and it refers to the state of the atmosphere at any given.
1 November 2007 Class #18.  HW #4 handed out today; due Tues Nov 13  Midterms will be returned on Tues  Observing tonight  9:00pm on the roof of Sterling.
Astro 18 – Section Week 2 EM Spectrum. ElectroMagnetic Radiation Energy moves in waves with electrical and magnetic components Energy moves in waves with.
Figure 1 Figure 8 Figure 9Figure 10 Altitude resolved mid-IR transmission of H 2 O, CH 4 and CO 2 at Mauna Loa Anika Guha Atmospheric Chemistry Division,
The Atmosphere: Structure & Temperature. Atmosphere Characteristics Weather is constantly changing, and it refers to the state of the atmosphere at any.
Saturn’s Auroras from the Cassini Ultraviolet Imaging Spectrograph Wayne Pryor Robert West Ian Stewart Don Shemansky Joseph Ajello Larry Esposito Joshua.
Infrared Spectroscopy (and the Cassini Composite Infrared spectrometer) Adam Ginsburg September 25, 2007.
Infrared spectroscopy of planetological molecules Isabelle Kleiner Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA), Créteil, France.
Weather and Climate Weather and Climate are Two Different Things
INFRARED CROSS SECTIONS OF HOT HYDROCARBONS
G. Mevi1,2, G. Muscari1, P. P. Bertagnolio1, I. Fiorucci1
Planetary Models for Herschel
UVIS Saturn Atmosphere Occultation Prospectus
Detection of H2O Vapor in AFGL 2591
Saturn upper atmosphere structure
Atmosphere Characteristics
SPICA for Transiting Exoplanets: Which SPICA instruments are useful?
Chapter 10.1 Planetary Atmospheres
Oxygen: Stratosphere, Mesosphere and Thermosphere Part-3
The Layered Atmosphere:
Presentation transcript:

IGRINS Science Workshop High Spectral Resolution Mid- Infrared Spectroscopy as a Probe of the Physical State of Planetary Atmospheres August 26, 2010

IGRINS Science Workshop Advantages of High Spectral Resolution Increased sensitivity to unresolved spectral features (changes linearly with resolving power) Increases spectral separation of observed emission or absorption features allowing for unique identifications of a multitude of molecular features when molecular rotation-vibration bands overlap. Increases the amount of open spectral space to observation by reducing blending and increasing separation of telluric absorption features. The line shape of resolved spectral features can be use to retrieve information on velocity of the gas (compact H 2 regions, galaxies, etc), information on vertical variation of temperature or abundance of molecules in a planetary atmosphere, or the ability to separate distinct clouds of gas along a given line of sight.

IGRINS Science Workshop TEXES: Texas Echelon Cross Echelle Spectrograph Operates between 5 and 25  m A ground based prototype for EXES, an instrument to be flown on SOFIA

IGRINS Science Workshop inches long 0.3 inch groove spacing 0.03 inch groove height 0.3” Echelon Grating

IGRINS Science Workshop T.K. Greathouse J.I. Moses J.H. Lacy M.J. Richter NASA/JPL/Space Science Institute Probing Stratospheric Chemistry, Energetics, and Dynamics. A Detailed Study of Giant Planet Stratospheres

IGRINS Science Workshop Pressure (bar) Temperature (Kelvin) Troposphere Stratosphere Thermosphere Tropopause Mesosphere Mesopause Stratopause General Atmospheric Structure

IGRINS Science Workshop Process Dependencies Stratospheric Temperatures  Chemistry  Latitude?  Season?  Insolation  Latitude  Season  Solar Flux  Molecular Abundances  Latitude?  Season?  Dynamic Mixing?  Heating  Aerosols  Chemistry  Insolation  Advection?  Cooling  Molecular Abundances  Chemistry  Advection?

IGRINS Science Workshop Moses et al. 2000, Icarus. Question: What molecules exist in the stratosphere?

IGRINS Science Workshop Using Doppler Shifts for Unambiguous Detection of C 3 H 8 First Detection of Propane on Saturn -20  10  Latitude -80  10  Latitude

IGRINS Science Workshop ISO Schulz et al First Detections of C 2 H 4 in Neptune

IGRINS Science Workshop A Second Detection AKARI data Fletcher et al. 2010

IGRINS Science Workshop The First Spectrally Resolved Detection of C 2 H 4 on Neptune

IGRINS Science Workshop Spectral Line Separation The Unambiguous Detection of C 3 H 8 Propane on Titan Roe et al Propane Measure weak lines Measure features in crowded spectral regions

IGRINS Science Workshop Seasonal Studies

IGRINS Science Workshop Temperature Retrievals Using thermal emission spectra to retrieve temperatures requires knowledge of mixing ratio of observed molecule. Methane serves this purpose. Homogeneously mixed vertically and horizontally we can use this useful molecule as a thermometer.

Courtesy Glenn Orton southern winter southern spring southern summer

IGRINS Science Workshop CH 4 emission from –80° latitude

IGRINS Science Workshop Temperatures from

IGRINS Science Workshop

IGRINS Science Workshop

IGRINS Science Workshop C

IGRINS Science Workshop Ethane Spectrum with Missing Features

IGRINS Science Workshop A Few Project Ideas for IGRINS Auroral studies on Jupiter –IGRINS gives access the simultaneous acquisition of H 2 and H 3 + emission features. Cloud elevation studies on Saturn and Jupiter. Occultation observations –Very good probe of CH 4 vertical density distribution. Comet Observations Kuiper belt objects probably best left to GMTNIRS

IGRINS Science Workshop